Caution: fresh snowdrifts. Wet loose-snow avalanches possible on very steep sunny slopes.
Due to light-to-moderate southerly winds, fresh snowdrift accumulations have been generated esp. in ridgeline terrain. The fresh drifts are small but often prone to triggering.
Due to daytime warming and solar radiation, increasingly frequent generally wet loose-snow avalanches are possible, esp. on extremely steep sunny slopes. Avalanches are triggerable by persons in the weak old snow, esp. on W/N/E facng slopes above 1800m, releases sometimes medium-sized. Due to light to moderate southerly winds, mostly small snowdrift accumulations are being generated, esp. on ridgeline slopes.
Snowpack
dp.10: springtime scenario dp.1: deep persistent weak layer
Due to southerly winds, small snowdrift accumulations will be generated. Fresh drifts lie deposited esp. on shady slopes atop weak layers. Sunny slopes: Due to low temperatures and low air moisture, a surface crust forms during the nocturnal hours. Solar radiation and daytime warmth lead to significantly moister snowpack, esp. on extremely steep slopes. Shady slopes: inside the snowpack are expansively metamorphosed (faceted) weak layers, esp on W/N/E facing slopes above 1800m. The old snowpack is expansively metamorphosed (faceted) on the surface. Due to southerly winds, small snowdrift accumulations are being generated. Winds are transporting only small amounts of snow. Fresh snowdrift accumulations lie deposited esp. on shady slopes atop soft layers.
Tendency
Danger level
Favorable avalanche situation
Due to solar radiation, increasingly frequent generally small-sized wet loose-snow avalanches are anticipated, esp. on extremely steep sunny slopes. Avalanches are triggerable by persons esp. by large addtional loading on NW/N/NE facing slopes above 2000m, releases mostly small.
Snowpack
dp.10: springtime scenario
Sunny slopes: Due to low temperatures and low air moisture, a surface crust forms during the nocturnal hours. Solar radiation and daytime warmth lead to significantly moister snowpack, esp. on extremely steep slopes. Shady slopes: inside the snowpack are expansively metamorphosed (faceted) weak layers, esp on W/N/E facing slopes above 1800m. The old snowpack is expansively metamorphosed (faceted) on the surface.
Tendency
Danger level
2200m
Avalanche Problem
Persistent weak layer
2200m
Wet snow
2800m
Caution: weak layers in old snow.
Due to light-to-moderate southerly winds, fresh snowdrift accumulations have been generated esp. in ridgeline terrain. The fresh drifts are small but often prone to triggering.
Due to daytime warming and solar radiation, increasingly frequent generally wet loose-snow avalanches are possible, esp. on extremely steep sunny slopes. Avalanches are triggerable by persons in the weak old snow, esp. on W/N/E facng slopes, releases usually small-sized. Due to light to moderate southerly winds, mostly small snowdrift accumulations are being generated, esp. on ridgeline slopes above 2200m.
Snowpack
dp.10: springtime scenario dp.1: deep persistent weak layer
Due to southerly winds, small snowdrift accumulations will be generated. Fresh drifts lie deposited esp. on shady slopes atop weak layers. Sunny slopes: Due to low temperatures and low air moisture, a surface crust forms during the nocturnal hours. Solar radiation and daytime warmth lead to significantly moister snowpack, esp. on extremely steep slopes. Shady slopes: inside the snowpack are expansively metamorphosed (faceted) weak layers, esp on W/N/E facing slopes above 2200m. The old snowpack is expansively metamorphosed (faceted) on the surface.
